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snowdgtv.cpp
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snowdgtv.cpp
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//copied from snowdgtv.f90
//_# 6.6.13
# include "uebpgdecls.h"
//**********************************************************************************************
//
// Copyright (C) 2012 David Tarboton, Utah State University, [email protected]. http://hydrology.usu.edu/dtarb
//
// This file is part of UEB.
//
// UEB is open source software: you can redistribute it and/or modify it under the terms of the
// MIT Open Source License as published by the Open Source Initiative https://opensource.org/licenses/MIT.
//
// Permission is hereby granted, free of charge, to any person obtaining a copy
// of this software and associated documentation files (the "Software"), to deal
// in the Software without restriction, including without limitation the rights
// to use, copy, modify, merge, publish, distribute, sublicense, and/or sell
// copies of the Software, and to permit persons to whom the Software is
// furnished to do so, subject to the following conditions:
//
// The above copyright notice and this permission notice shall be included in all
// copies or substantial portions of the Software.
//
// THE SOFTWARE IS PROVIDED "AS IS", WITHOUT WARRANTY OF ANY KIND, EXPRESS OR
// IMPLIED, INCLUDING BUT NOT LIMITED TO THE WARRANTIES OF MERCHANTABILITY,
// FITNESS FOR A PARTICULAR PURPOSE AND NONINFRINGEMENT. IN NO EVENT SHALL THE
// AUTHORS OR COPYRIGHT HOLDERS BE LIABLE FOR ANY CLAIM, DAMAGES OR OTHER
// LIABILITY, WHETHER IN AN ACTION OF CONTRACT, TORT OR OTHERWISE, ARISING FROM,
// OUT OF OR IN CONNECTION WITH THE SOFTWARE OR THE USE OR OTHER DEALINGS IN THE
// SOFTWARE.
//
// If you wish to use or incorporate this program (or parts of it) into
// other software that does not meet the MIT Open Source License
// conditions contact the author to request permission.
// David G. Tarboton
// Utah State University
// 8200 Old Main Hill
// Logan, UT 84322-8200
// USA
// http://hydrology.edu/dtarb/
// email: [email protected]
//
//**********************************************************************************************
// Definitions
// dt time step in hours
// nt number of time steps
// input -- input forcing
// input(1,*) air temperature (C)
// input(2,*) precipitation (m/hr)
// input(3,*) wind speed (m/s)
// input(4,*) relative humidity (on a 0-1 scale)
// input(5,*) incoming short wave (kJ/m^2/h)
// input(6,*) net radiation (kJ/m^2/h)
// input(7,*) Cosine of Zenith angle
// SITEV -- site variables
// site variables (1-5)
// sitev(1) drift factor (No detailed information give 1)
// sitev(2) air pressure (Pa)
// sitev(3) ground heat flux Kj/m^2/hr (3.6 = 1 W/m^2)
// sitev(4) albedo extinction parameter (m)
// STATEV
// statev(1) Snow Energy Content (KJ/m^2)
// statev(2) Snow Water Equivalent (m) relative to T = 0 C solid phase
// statev(4) Canopy Snow Water Equivalent (m) relative to T = 0 C solid phase
// statev(3) Dimensionless age of snow surface (or albedo - depending on flag 4)
// statev(5) Refreezing depth (m) used as refdepth
// statev(6) Refreezing depth (m) used as totalrefdepth
// totalrefdepth is a misnomer. These are the same quantity - the refreezing depth. They are repeated because
// when refdepth exceeds the diurnal penetration depth it is set to 0 to tell the code to use the regular
// surface temperature functions while totalrefdepth is only reset to 0 when there is actual melt generated
// or energy content becomes negative indicating freezing of all liquid phase. This ensures that the regular
// surface temperature functions persist when there is liquid water present but the refreezing front has penetrated
// to depth greater than diurnal temperature fluctuations.
// TsPrevday(1:nstepday) Surface temperature over the last 24 hours
// TavePrevday(1:nstepday) Depth average te
// Imperature over the last 24 hours
//
// PARAM -- snowmelt model parameters (see below)
// iflag -- flags
// iflag(1) 0=radiation is shortwave in col 5 and longwave in col 6, else = net radiation in column 7
// iflag(2) no 0 (/yes 1) printing
// iflag(3) unit to which to print
// iflag(4) how albedo calculations are done (a value 1 means albedo is calculated, otherwise statev(3) is albedo
// iflag(5) model option for surface temperature approximation
// 1) the Simple Gradient, almost the same as Original UEB,
// 2) Simple Gradient approach with shallow snow correction.
// 3) The classical force-restore approach.
// 4) Modified force-restore approach.
// cump,cume,cummr -- cumulative precipitation (with df), cumulative evaporation, cumulative melt over time step in m
// outv -- output variables
// outv(1)=prain rain m/hr
// outv(2)=ps snow m/hr
// outv(3)=a albedo
// outv(4)=qh sensible heat (kJ/m2/hr)
// outv(5)=qe latent heat (kJ/m2/hr)
// outv(6)=e sublimation m/hr
// outv(7)=mr melt outflow m/hr
// outv(8)=qm heat advected with melt
// outv(9)=q Energy rate of change (kJ/m2/hr)
// outv(10)=fm Mass rate of change (m/hr)
// outv(11)=tave Average temperature (C)
// outv(12)=tsurf Surface temperature C
// outv(13)=qnet Net Radiation (kJ/m2/hr)
// outv(14)=smelt Surface melt m/hr
//
//yjs Note: in this subroutine, the outv is an array which passes value to this subroutine and back to the snow
//yjs drive program. The Outv(9) and outv(10) pass the daily average snowpack temperature and daily
//yjs snow surface temperature to this subroutine but pass the Qin total and combined mass fluxes
//yjs back. //
void SNOWUEB2(float dt, float *input, float *sitev, float *statev, float *tsprevday, float *taveprevday, int &nstepday, float *param, int *iflag,
float &cump, float &cumes, float &cumEc, float &cumMr, float &cumGM, float &cumEg,float *outv, float *mtime ,float atff, float cf, float *OutArr)
{
const int niv = 8;
int pflag, iradfl;
//FILE *outUnit;
// For canopy variables
float AvailableSnow, RemainingAvailableWater;
//CHANGES TO ACCOMODATE GLACIER
float WGT; // WGT=WATER EQUIVALENT GLACIER THICKNESS
int iTsMethod; //yjs Add model time initialization 09/19/2000
int windfl;
float SWIT,SWISM, SWIR,SWIGM;
//definition added--didn't exit in the forrtran version 5.6.13
float refDepth, totalRefDepth, Us_old, refDepth_old;
float RRHOI, RRHO ,RID ,rhom;
float Ta, P, V, RH, Qsi, Qli, Qnetob, cosZen, Tave;
//int snowdgtvariteflag = 0;
float Ps, Pr, Alb/*previously A*/, Rhofs, S;
//outputs from Predictor corrector
float Tc, QHc, QEc, Ec, Qpc, Qmc, Mc, FMc, intc, Inmax, ieff, Ur, Taufb, Taufd, Qsib, Qsid, Taub, Taud, Qsnc, Qsns, Qlnc, Qlns, Rkinc, Rkinsc, Vz, Tac;
// Just for testing (outputs from predictor corre)
float QHs, QEs, Es, QPs, Mr, QMs, Q, FM, TSURFs, Tavepc, Qnet, smelt, Qlis;
//####***TGBC_6. 5.13
// Parameters
float Tr=param[0], // Temperature above which all is rain [3 C],
Ts=param[1], // Temperature below which all is snow [-1 C],
Ems=param[2], // emmissivity of snow [nominally 0.99],
cg =param[3], // Ground heat capacity [nominally 2.09 KJ/kg/C],
z=param[4], // Nominal meas. height for air temp. and humidity [2m],
zo=param[5], // Surface aerodynamic roughness [m],
rho=param[6], // Snow Density [Nominally 450 kg/m^3],
rhog=param[7], // Soil Density [nominally 1700 kg/m^3],
lc=param[8], // Liquid holding capacity of snow [0.05],
ks=param[9], // Snow Saturated hydraulic conductivity [20 m/hr],
de=param[10], // Thermally active depth of soil [0.1 m],
abg=param[11], // Bare ground albedo [0.25],
avo=param[12], // Visual new snow albedo [0.95],
anir0=param[13], // NIR new snow albedo [0.65],
lans= param[14], // the thermal conductivity of fresh [dry], snow [0.0576 kJ/m/k/hr], [Vinod// 0.36 Ref: Snow and Climate :Richard L Armstrong and Eric Brun ],
lang= param[15], // the thermal conductivity of soil [:9.68 kJ/m/k/hr], [TK of ice or wet soil[2.22~ 3.48W/m/k],:Vinod],
wlf= param[16], // Low frequency fluctuation in deep snow/soil layer [1/4 w1 = 0.0654 radian/hr],
rd1= param[17], // Apmlitude correction coefficient of heat conduction [1],
fstab=param[18], // Stability correction control parameter 0 = no corrections, 1 = full corrections
Tref=param[19], // Reference temperature of soil layer in ground heat calculation input
dNewS=param[20], // The threshold depth of for new snow [0.001 m],
gsurf=param[21], // The fraction of surface melt that runs off [e.g. from a glacier],
// 7 Parameters added for canopy
EmC = param[22], // Emissivity of canopy
alpha = param[23], // Scattering coefficient for solar radiation
alphaL = param[24], // Scattering coefficient for long wave radiation
G = param[25], // leaf orientation with respect to zenith angle
Uc = param[26], // Unloading rate coefficient [Per hour], [Hedstrom and pomeroy, 1998],
as = param[27], // Fraction of extraterrestaial radiation on cloudy day,Shuttleworth [1993],
bs = param[28], // [as+bs],:Fraction of extraterrestaial radiation on clear day, Shuttleworth [1993],
Lambda = param[29], // Ratio of direct atm radiation to diffuse,worked out from Dingman [1993],
Rimax = param[30], // Maximum value of Richardsion number for stability corretion
Wcoeff = param[31]; // Wind decay coefficient for the forest
// Some initializations
Rkinc=0.0;
Tac=0.0;
// State Variables - These serve as initial conditions
float Us = statev[0], // Snow Energy Content [KJ/m^2];
Ws = statev[1], // Snow Water Equivalent [m]; relative to T = 0 C solid phase
Wc = statev[3]; // Added for canopy
/*if(snowdgtvariteflag == 1)
for (int ki=0;ki<4; ki++)
cout<<statev[ki]<<endl;
cout<<Ws<<" "<<Wc<<endl;
*/
if(Us <= 0.0)
{
refDepth = 0.0;
totalRefDepth = 0.0;
}
else
{
refDepth = statev[4];
totalRefDepth = statev[5];
}
// Save Old Value 07/23/01
Us_old = Us;
refDepth_old = refDepth;
// Site Variables
float dF = sitev[0], // Drift factor
APr= sitev[1], // Atmospheric Pressure [Pa],
qg = sitev[2], // Ground heat flux [KJ/m^2/hr], This is more logically an
// input variable,but is put here because it is never known at each
// time step. Usually it will be assigned a value 0.
Aep= sitev[3], // Albedo extinction parameter to smooth
// transition of albedo when snow is shallow. Depends on Veg. height [m],
// 7 Site Variables added for canopy
Cc = sitev[4], // Canopy Coverage
Hcan = sitev[5], // Canopy height
LAI = sitev[6], // Leaf Area Index
Sbar = sitev[7], // Maximum snow load held per unit branch area[Kg/m2 for Pine],
Ycage = sitev[8]; // Parameters for wind speed transformation
// Ycage=1 for young pine Should be in parameters
// Ycage=2 for Leafed deciduous
// Ycage=3 for Old pine with logn stems (Paw U and Meyers, 1987)
// Requires for wind speed transformation
// Control flags
iradfl= iflag[0];
pflag = iflag[1];
//ounit = iflag[2]; //iflag(4) albedo caculation
iTsMethod = iflag[4]; // the method to approximate the surface temperature
// 1 normal old snow melt model
// 2 revised direct gradient method (New method for ke) and qe
// 3 force restore approach
// 4 modified force restore approach
windfl = iflag[5];
// Model time step information
float yy = mtime[0],
mm = mtime[1],
dd = mtime[2],
hr = mtime[3];
//**************************************************
// Different densities and their ratio
RRHOI= Rho_i/Rho_w;
RRHO = rho/Rho_w;
RID = 1.0/RRHO-1.0/RRHOI; //used to compute melt water flux (Fmelt)
rhom = lc*rho;
// for Gracier melting calculation
if((sitev[9] == 0) || (sitev[9] == 3))
WGT=0.0;
else
WGT=1.0;
Ws = Ws+WGT;
// loop over nt removed here because UEBGrid makes single call to this function
//#_5.6.13
// DO 2 i = 1,nt
// Input variables
Ta =input[0]; // Air temperature input [Degrees C];
P =input[1]; // Precipitation rate input [m/hr];
V =input[2]; // Wind Speed [m/s];
RH =input[3]; // Relative humidity [fraction 0-1];
// if[iradfl.eq.0];THEN // input is incoming short and longwave
Qsi=input[4]; // Incoming shortwave radiation [KJ/m^2/hr];
Qli=input[5]; // Incoming longwave radiation [KJ/m^2/hr];
// ELSE
Qnetob = input[6]; // Net allwave radiation [KJ/m^2/hr];
// ENDIF
cosZen = input[7]; // Cos[angle between direct sunlight and surface normal];
// Representative value over time step used in albedo calculation.
// We neglect the difference between direct and diffuse albedo.
//DGT Daily average temperatures handled internally so that multiple time steps will work
Tssk_ave = daily_ave(tsprevday, nstepday, -100.0) + T_k; // (K) Surface temperature average over last 24 hours
Tsavek_ave = daily_ave(taveprevday, nstepday, -100.0) + T_k; // (K) Depth averaged temperature average over last 24 hours
// if(snowdgtvariteflag == 1)
//cout<<Tssk_ave<<" "<<Tsavek_ave<<endl;
Tssk_old = tsprevday[nstepday-1] + T_k; // (C) Surface temperature from previous time step
Tsavek_old = taveprevday[nstepday-1] + T_k; // (C) Average temperature from previous time step
// ifany of these variables are out of range due to any problem set them back to freezing
if(Tssk_old < 0)
{
if(snowdgtvariteflag == 1)
cout<<"Invalid previous time step surface temperature set to 273 K"<<Tssk_old<<endl;
Tssk_old = T_k;
}
if(Tsavek_old < 0)
{
if(snowdgtvariteflag == 1)
cout<<"Invalid previous time step average temperature set to 273 K"<<Tsavek_old<<endl;
Tsavek_old = T_k;
}
if(Tssk_ave < 0)
{
if(snowdgtvariteflag == 1)
cout<<"Invalid last 24 hr average surface temperature set to 273 K"<<Tssk_ave<<endl;
Tssk_ave = T_k;
}
if(Tsavek_ave < 0)
{
if(snowdgtvariteflag == 1)
cout<<"Invalid last 24 hr average temperature set to 273 K"<<Tsavek_ave<<endl;
Tsavek_ave = T_k;
}
// Separate rain and snow
Ps = PARTSNOW(P,Ta,Tr,Ts);
Pr = P - Ps;
// Increase precipitation as snow by drift multiplication factor
Ps = Ps * dF;
// Calculate Albedo
// for Gracier melting calculation
if(iflag[3] == 1)
// if(SITEV(10) .EQ. 0 .OR. SITEV(10) .EQ. 3)THEN
Alb = ALBEDO(statev[2], cosZen, (Ws-WGT)/RRHO, Aep, abg, avo, anir0); // Snow depth (Ws/RRho)
// ELSE // Use of this albedo throughout time step neglects the
// A=albedo(statev(3),cosZen,(Ws-WGT)/RRHO,aep,abg,avo,anir0)// changes due to new snow within a time step.o
// ENDIF
else
Alb = statev[2];
//************ Maximum Interception, Literature ************************
// This model assumes that rainfall interception and thoroughfall occurs in a similar way that snowfall interception and unloading does.
// However this model is not suitable to model the rainfall interception and throughfall
Rhofs = 67.92 + 51.25 * exp(Ta/2.59); // Density of fresh snow from air temp, Army Corps 1956.
S = Sbar * (0.27 + 46/Rhofs ); // canopy holding capacity depends on density of snow (Headstrom and Pomeroy (1998))
Inmax = S * LAI; // kg/m2 =lit/m2 = .001m3/m2=.001 m =1/1000 m ()
if(Cc > 0)
Inmax = Inmax/1000 * Cc; // convert to m for per sq m of canopy
else
Inmax = 0;
//if(snowdgtvariteflag == 1)
//cout<<LAI<<" "<<Cc<<" "<<" "<<Sbar<<" "<<Rhofs<<" "<<S<<" "<<Inmax<<endl;
// Call predictor corrector subroutine to do all the work for Canopy
PREDICORRc(Us,Ws,Wc,Alb,dt,RID,P,Pr,Ps,Ta,V,RH,Qsi,Qli,atff, cosZen,EmC,Ems,param,sitev,iradfl,Qnetob,iTsMethod,mtime,
Tc,QHc,QEc,Ec,Qpc,Qmc,Mc,FMc,intc,Inmax,ieff,Ur, cf,Taufb,Taufd,Qsib,Qsid,Taub,Taud,Qsnc,Qsns,Qlnc,Qlns,Rkinc,
Rkinsc,Vz,Tac, QHs, QEs, Es, QPs, Mr, QMs, Q, FM, TSURFs, Tavepc, Qnet, refDepth, totalRefDepth, smelt, gsurf,Qlis);
// DGT 4/2/05 Despite all checks in predicor It can (and does) occur that we still have Us so large that it results in tavepc greater than 0, which implies that all the
// snow is liquid. In these cases - just force the snow to disappear and add the energy involved to Qm.
Tave = TAVG(Us,Ws,Rho_w,C_s,T_0,rhog,de,cg,H_f); // this call necessary to keep track of average internal temperature used in some surface energy algorithms.
if(snowdgtvariteflag == 1)
cout<<Tave<<endl;
if(Tave > 0) // all is liquid so snow must disappear
{
Mr = Mr+Ws/dt;
QMs = QMs+Ws/dt*Rho_w*H_f;
Q = Q-Ws/dt*Rho_w*H_f;
Us = Us-Ws/dt*Rho_w*H_f;
Ws = 0.0;
}
// since Us, Ws was changed need T_0 re-evaluate Tave
Tave = TAVG(Us,Ws,Rho_w,C_s,T_0,rhog,de,cg,H_f);
//if(snowdgtvariteflag == 1)cout<<Tave<<endl;
// DGT 7/25/05 T_0 guard against unreasonable Us when there is no snow do not allow bulk temperature T_0 go above 10 C
if(Tave > 10)
{
Us=rhog*de*cg*10.0;
Tave = 10.0;
}
// Update snow surface age based on snowfall in time step
if(iflag[3] ==1)
AGESN(statev[2],dt,Ps,TSURFs,T_k,dNewS);
// if(snowdgtvariteflag == 1)
//cout<<statev[2]<<endl;
// 2013 - Introduced glacier substrate into model
// Partition melt outflow into the portion that is from rain, snow and glacier
// Inputs are condensation (C=max(-Es,0)), precipitation as rain (pr) and precipitation as snow (Ps)
// Outputs are melt (Mr) and sublimation (Sub=Max(Es,0))
// DW is change in snow water equivalent (positive if decrease)
// DG is change in glacier (positive if decrease)
// Mass balance
// DW+DG=Mr+Sub-Pr-Ps-C
// In the case of snow left on the ground/glacier - any rain is assumed to have added to the snow
float SnowLeft = findMax(Ws-WGT,0.0);
float DW = (statev[1] - SnowLeft)/dt; // change in seasonal snow rate
// Reduction in snow storage is snow at the beginning minus the snow at the end in excess of glacier. Can be negative if snow increases
float DG = findMax(WGT-Ws,0.0)/dt; // Reduction in glacier storage rate
float R, MSX, MRX, Ms, MG, Eglacier;
if(SnowLeft > 0.)
{
R=0.0; // No outflow due to rain
// Inequalities that hold
// 0<= Ms <= Ps+Pr+C+DW
// 0<= MG <= DG
// The slack in these inequalities is due to Sub
// Compute Ms and MG using proportioning
MSX = Ps+Pr+DW+ findMax(-Es,0.0); // Maximum melt contrib from snow. Note that condensation is taken to add to snow as is rain
MRX = MSX+DG; // Maximum melt overall
// Mr is less than MRX due to sublimation losses. Do the rain proportioning accordingly
if(MRX <= 0.0)
{
Ms=0.0;
MG=0.0;
}
else
{
Ms=Mr*MSX/MRX;
MG=Mr*DG/MRX;
}
}
else
{// The case where all seasonal snow is gone and precipitation may contribute to total outflow
// Inequalities that hold
// 0<= Ms <= Ps+C+DW
// 0<= R <= Pr
// 0<= MG <= DG
// The slack in these inequalities is due to Sub. Note that here Pr may contribute to R but that C is still put to snow
MSX = Ps+DW+ findMax(-Es,0.0); // Maximum melt contrib from snow. Note that condensation is taken to add to snow as is rain
MRX = MSX+DG+Pr; // Maximum melt overall
if(MRX <= 0.0)
{
Ms=0.0;
R=0.0;
MG=0.0;
}
else
{
Ms=Mr*MSX/MRX;
R=Mr*Pr/MRX;
MG=Mr*DG/MRX;
}
}
Eglacier=DG-MG;
SWISM=Ms;
SWIGM=MG;
SWIR=R;
SWIT=Mr;
if(Ws < WGT) // There was glacier melt
Ws=0.0; // Reset
else // Here ws is greater than the glacier thickness so no glacier melt
Ws=Ws-WGT;
/* commented out 10.2.13 relacing with the above
// Partition of melt outflow between rain and snow melt for non glacier case
if(Ws > 0)
{
SWIR = 0;
SWISM = Mr;
}
else // This else case is never entered for glaciers because the entire WGT is not melted in one time step
{
AvailableSnow = (Ps + statev[1]/dt);
SWISM = findMin(AvailableSnow,Mr); // This bounds snow surface melt by the available snow - the balance is due T_0 rain
SWIR = Mr-SWISM;
}
// Correction T_0 partition T_0 account for presence of glaciers
if(Ws < WGT) // There was glacier melt
{
AvailableSnow = (Ps+statev[1]/dt);
SWISM = findMin(AvailableSnow,Mr); // This bounds snow surface melt by the available snow - the balance is due T_0 rain
RemainingAvailableWater = Mr-SWISM; // This is the remaining melt T_0 allocate
SWIGM = findMin(RemainingAvailableWater,(WGT-Ws)/dt);
SWIR = Mr-SWISM-SWIGM;
Ws = 0; // Reset
}
else // Here ws is greater than the glacier thickness so no glacier melt
{
Ws = Ws - WGT;
SWIGM = 0;
}
// SWIT=Mr+SWIGM // DGT 2/22/13. THis seems wrong
SWIT = Mr; // The total is always Mr */
// accumulate for mass balance
cump = cump+(Ps+Pr)*dt;
cumes = cumes+Es*dt;
cumEc = cumEc+Ec*dt; // Evaporation from canopy
cumMr = cumMr+Mr*dt; // canopy melt not added
cumGM = cumGM+SWIGM*dt; // Cumulative glacier melt
cumEg= cumEg+Eglacier*dt;
// yjs update the total depth of the refreezing depth in the snow pack according the the refreezing depth at time step and the positive energy input. 07/22/01
// DGT's revised logic 1/13/05
if(lc > 0 )
{
if(refDepth > 0)
totalRefDepth = refDepth; // ifrefreezing depth increases totalRefDepth keeps track
else
{ // here refDepth has gone T_0 0 somehow
if( (Mr > 0) || (Us > Us_old && Us > 0)) // ifthere is melt or an increase in energy refDepth is reset
totalRefDepth = 0.0;
}
}
else if ( (Mr > 0) || (Us > Us_old && Us > 0)) // Here lc=0. ifthere is melt or an increase in energy refDepth is reset
totalRefDepth =0.0; // This is likely redundant because iflc=0 then there is no meltwater T_0 refreeze
if(totalRefDepth < 0)
totalRefDepth = 0.0;
//yjs update tsbackup and tavebackup
for(int ii = 0; ii< nstepday-1; ++ii)
{
tsprevday[ii] = tsprevday[ii+1];
taveprevday[ii]= taveprevday[ii+1];
}
tsprevday[nstepday-1] = TSURFs;
taveprevday[nstepday-1]= Tave;
OutArr[0] = Us;
OutArr[1] = Ws;
OutArr[2] = statev[2];
OutArr[3] = Pr;
OutArr[4]=Ps;
OutArr[5]=Alb;
OutArr[6]=QHs;
OutArr[7]=QEs;
OutArr[8]= Es;
OutArr[9]=SWIT;
OutArr[10]=QMs;
OutArr[11]=Q;
OutArr[12]= FM;
OutArr[13]=Tave;
OutArr[14]=TSURFs;
OutArr[15]=cump;
OutArr[16]=cumes;
OutArr[17]=cumMr;
OutArr[18]=Qnet;
OutArr[19]=smelt;
OutArr[20]=refDepth;
OutArr[21]=totalRefDepth;
OutArr[22]=cf;
OutArr[23]=Taufb;
OutArr[24]=Taufd;
OutArr[25]=Qsib;
OutArr[26]=Qsid;
OutArr[27]=Taub;
OutArr[28]=Taud;
OutArr[29]=Qsns;
OutArr[30]=Qsnc;
OutArr[31]=Qlns;
OutArr[32]=Qlnc ;
OutArr[33]=Vz;
OutArr[34]=Rkinsc;
OutArr[35]=Rkinc;
OutArr[36]=Inmax;
OutArr[37]=intc;
OutArr[38]=ieff;
OutArr[39]=Ur;
OutArr[40]=Wc;
OutArr[41]=Tc;
OutArr[42]=Tac;
OutArr[43]=QHc;
OutArr[44]=QEc;
OutArr[45]=Ec;
OutArr[46]=Qpc;
OutArr[47]=Qmc;
OutArr[48]=Mc;
OutArr[49]=FMc;
OutArr[50]=SWIGM;
OutArr[51]=SWISM;
OutArr[52]=SWIR;
//2 continue
statev[0]=Us;
statev[1]=Ws;
statev[4]=refDepth;
statev[5]=totalRefDepth;
statev[3]= Wc ; // Added vinod
outv[0]=Pr;
outv[1]=Ps;
outv[2]=Alb;
outv[3]=QHs;
outv[4]=QEs;
outv[5]=Es;
outv[6]=Mr;
outv[7]=QMs;
outv[8]=Q;
outv[9]=FM;
outv[10]=Tave;
outv[11]=TSURFs;
outv[12]=Qnet;
outv[13]=smelt; // dgt 5/4/04
return;
}
//************************ Predictor CORRECTOR ***********************************
void PREDICORRc ( float &Us, float &Ws, float &Wc, float Alb, float dt, float rid, float P, float Pr, float Ps, float Ta, float V, float RH, float Qsi, float Qli,
float atff, float cosZen, float EmC, float Ems, float *param, float *sitev, int iradfl, float Qnetob, int iTsMethod, float *mtime,
// Following variables are output
float &Tc, float &QHc, float &QEc, float &Ec, float &Qpc, float &Qmc, float &Mc, float &FMc,float &intc, float &Inmax, float &ieff, float &Ur, float &Cf,
float &Taufb, float &Taufd, float &Qsib, float &Qsid, float &Taub,float &Taud, float &Qsnc, float &Qsns, float &Qlnc, float &Qlns, float &Rkinc, float &Rkinsc, float &Vz, float &Tac,
// Just for testing
float &QHs, float &QEs,float &Es, float &QPs, float &MR, float &QMs, float &Q,float &FM, float &TSURFs, float &tave, float &Qnet, float &refDepth, float &totalRefDepth, float &smelt,
float &gsurf, float &Qlis )
{
float LAI, int1, Mc1, Mr1,Apr, Cc;
float smeltC, Wc1, FMc1,Ur1,Ec1,Tc1,Ws1,Us1,Q1,FM1,QHs1,QEs1, Es1, smelt1, TSURFs1, QMs1, Qnet1, Wc2, Ws2, Us2, Es2;
float Ae, rlf, r;
float WGT = 1.0;
Apr = sitev[1];
Cc = sitev[4];
LAI = sitev[6];
QFMc(Us,Ws,Wc,Alb,dt,rid,P,Pr,Ps,Ta,V,RH,Qsi,atff,Qli, cosZen,EmC,Ems,param,sitev,iradfl,Qnetob,iTsMethod,mtime,
Tc,QHc,QEc,Ec,Qpc,QPs,Qmc,Mc,FMc,intc,Inmax,ieff,Ur, Cf,Taufb,Taufd,Qsib,Qsid,Taub,Taud,Qsnc,Qsns,Qlnc,Qlns,Rkinc,
Rkinsc,Vz,TSURFs,Tac, tave,Qnet,QHs,QEs,Es,MR,QMs,Q,FM,refDepth,totalRefDepth, smelt,smeltC);
// PREDICTOR FOR CANOPY SNOW
Wc1 = Wc + dt*FMc;
if(Wc1 < 0)
{
Wc1 = 0.0;
FMc = (Wc1- Wc)/dt;
Ur = findMax (0.0, (intc-FMc-Ec-Mc));
Ec = findMax(0.0,(intc-FMc-Mc-Ur));
Mc = (intc-FMc-Ec-Ur);
FM = Pr+Ps-intc+Ur+Mc-MR-Es; // int,ur,Mc added here
}
// Save values so that they can be averaged for output
FMc1 = FMc;
int1 = intc;
Ur1 = Ur;
Mc1 = Mc;
Ec1 = Ec;
Tc1 = Tc;
// PREDICTOR FOR SUB-CANOPY SNOW
Ws1 = Ws + dt*FM;
if(Ws1 < 0)
{
Ws1=0.0;
PREHELP(Ws1,Ws,dt,FM,0.0,1.0,Ps,Pr,Es,Rho_w,H_f,Q,QMs,MR,QEs, Hne_u);
}
Us1 = Us + dt*Q;
Q1 = Q;
FM1 = FM;
// Save values so that they can be averaged for output
QHs1 = QHs;
QEs1 = QEs;
Es1 = Es;
Mr1 = MR;
smelt1 =smelt; //cdgt 5/4/04 surface melt smelt
QMs1 = QMs;
TSURFs1 = TSURFs;
Qnet1 = Qnet;
if(snowdgtvariteflag3 == 1)
{
cout<<"\n Predictor: Us1, Ws1, Ts1, Q1, FM1 "<<endl;
cout<<" "<< Us1<<" "<< Ws1<<" "<<TSURFs1<<" "<<Q1<<" "<<FM1<<endl<<endl;
}
QFMc(Us1,Ws1,Wc1,Alb,dt,rid,P,Pr,Ps,Ta,V,RH,Qsi,atff,Qli, cosZen,EmC,Ems,param,sitev,iradfl,Qnetob,iTsMethod,mtime,
Tc,QHc,QEc,Ec,Qpc,QPs,Qmc,Mc,FMc,intc,Inmax,ieff,Ur, Cf,Taufb,Taufd,Qsib,Qsid,Taub,Taud,Qsnc,Qsns,Qlnc,Qlns,Rkinc,
Rkinsc,Vz,TSURFs,Tac, tave,Qnet,QHs,QEs,Es,MR,QMs,Q,FM,refDepth,totalRefDepth, smelt,smeltC);
// CORRECTOR FOR CANOPY SNOW
Wc2 = Wc + dt/2.0*(FMc1 + FMc);
if(Wc2 < 0)
{
Wc2 = 0.0;
FMc = (Wc2- Wc)/dt*2-FMc1;
Ur = findMax(0.,(intc-FMc-Ec-Mc));
Ec = findMax(0.,(intc-FMc-Mc-Ur));
Mc = (intc-FMc-Ec-Ur);
FM = Pr + Ps-intc+Ur+Mc-MR-Es; // int,ur,Mc added here
}
intc = (int1 +intc)/2;
Ur = (Ur1+Ur)/2;
Mc = (Mc1+Mc)/2;
Ec = (Ec1+Ec)/2; // But Mc and Ec don't change
Wc = Wc2;
Tc = (Tc1+ Tc)/2;
FMc = (FMc1+FMc)/2;
// CORRECTOR FOR SUB_CANOPY SNOW
Ws2 = Ws + dt/2.0*(FM1 + FM);
if(Ws2 < 0)
{
Ws2 = 0.0;
PREHELP(Ws2,Ws,dt,FM,FM1,2.0,Ps,Pr,Es,Rho_w,H_f,Q,QMs,MR,QEs,Hne_u);
}
Us2 = Us + dt/2.0*(Q1 + Q);
if(snowdgtvariteflag3 == 1)
{
cout<<"\n Corrector: Us2, Ws2, Ts, Q, FM "<<endl;
cout<<" "<< Us2<<" "<< Ws2<<" "<<TSURFs<<" "<<Q<<" "<<FM<<endl<<endl;
}
// iterate to convergence to enhance stability
int niter = 1, imax = 5;
while ((abs(Ws2-Ws1) > wtol || abs(Us2-Us1) > utol) && (niter < imax))
{
Ws1 = Ws2;
Us1 = Us2;
Wc1 = Wc2;
QFMc(Us1,Ws1,Wc1,Alb,dt,rid,P,Pr,Ps,Ta,V,RH,Qsi,atff,Qli, cosZen,EmC,Ems,param,sitev,iradfl,Qnetob,iTsMethod,mtime,
Tc,QHc,QEc,Ec,Qpc,QPs,Qmc,Mc,FMc,intc,Inmax,ieff,Ur, Cf,Taufb,Taufd,Qsib,Qsid,Taub,Taud,Qsnc,Qsns,Qlnc,Qlns,Rkinc,
Rkinsc,Vz,TSURFs,Tac, tave,Qnet,QHs,QEs,Es,MR,QMs,Q,FM,refDepth,totalRefDepth, smelt,smeltC);
// CORRECTOR FOR CANOPY SNOW AGAIN
Wc2 = Wc + dt/2.0*(FMc1 + FMc);
if(Wc2 < 0)
{
Wc2 = 0.0;
FMc = (Wc2- Wc)/dt*2-FMc1;
Ur = findMax(0.0,(intc-FMc-Ec-Mc));
Ec = findMax(0.0,(intc-FMc-Mc-Ur));
Mc = (intc-FMc-Ec-Ur);
FM = Pr+Ps-intc+Ur+Mc-MR-Es; // int,ur,Mc added here
// FM = FM+ (FMc-Ec)
}
intc = (int1 +intc)/2;
Ur = (Ur1+Ur)/2;
Mc = (Mc1+Mc)/2;
Ec = (Ec1+Ec)/2;
Wc = Wc2;
Tc = (Tc1+ Tc)/2;
FMc = (FMc1+FMc)/2;
//dgt 5/4/04 surface melt smelt
// corrector again
Ws2 = Ws + dt/2.0*(FM1 + FM);
if(Ws2 < 0)
{
Ws2 = 0.0;
PREHELP(Ws2,Ws,dt,FM,FM1,2.0,Ps,Pr,Es,Rho_w,H_f,Q,QMs,MR,QEs,Hne_u);
}
Us2 = Us + dt/2.0*(Q1 + Q);
niter++;
if(niter >= imax) // had * steps to converge now hit it. What follows is Alb fix to numerical instability that results from
{ // nonlinearity when the snowpack is shallow and melting rapidly. If convergence does not occur when the snowpack is not melting (Alb very
// rare thing) I just accept the predictor corrector solution. //
// Modified by DGT 7/27/05 to add complete meltout condition .The quantities that this changes are w2, ub2, MR and QMs
// The fix first checks whether the added energy is sufficient to melt the snow completely. ifthis is the case then the snow disappears.
// In other cases we assume that the liquid fraction of the snow remains constant. This to some extent bypasses the melt outflow estimates.
// ae is added energy during the time step.
Ae = (Q1+Q+QMs1+QMs)*0.5*dt; // This fix is only physically sensible under melting conditions and when ae is positive and there is snow
if((Us > 0) && (Ae > 0) && (Ws > 0))
{
Es2=(Es+Es1)*0.5; // This is the average sublimation
// Check liquid fraction with added energy. ifthis is greater than 1 then all snow melts .Otherwise implement Alb solution assuming that the liquid fraction remains constant
rlf=(Us+Ae)/(Rho_w*Ws*H_f);
if(rlf >= 1.0)
{
MR = Ws/dt+(Ps+Pr-Es2); // Here snow disappears
if(MR < 0 ) // Force this to not go negative. This can only occur if e2 is large compared to other terms. Setting w2=0 implicitly reduces e2.
MR = 0.0; // There is Alb resulting energy discrepancy due to Alb limitation on sublimation and latent heat flux
//This is ignored because once the snow is gone energy computations are not pertinent.
QMs=MR*Rho_w*H_f;
Ws2 = 0.0;
Us2 = Us + Ae - QMs*dt;
}
else // Determine the w/ub ratio at the beginning of the time step. Physically liquid fraction = ub/(Rho_w*w*H_f) and since Rho_w and H_f are constants
{ // keeping r=w/ub constant is equivalent to keeping liquid fraction constant. ifliquid fraction is constant this is constant.
r = Ws/Us; // Solve for ub2 and w2 that satisfy the three equations
// r=w2/ub2
// ub2=ub+Ae-Rho_w*H_f*MR*dt Energy balance the last term being the energy advected by melt
// w2=w+(Ps+prain-e2-MR)*dt Mass balance
// The unknowns in the above are ub2, w2 and m and the equations are linear. once the first eqn is multiplied by ub2, the solution is
Us2 = (Rho_w*H_f*(Ws+(Ps+Pr-Es2)*dt)-Ae-Us)/(Rho_w*H_f*r - 1);
Ws2=r*Us2;
if(Ws2 < 0) // Avoid negative W
Ws2 = 0.0;
MR = (Ws-Ws2)/dt -Es2 + Ps +Pr;
if(MR < 0 ) // Avoid negative MR
{
MR = 0.0;
Ws2 = Ws+ (Ps+Pr-Es2)/dt;
if(Ws2 < 0)
Ws2 = 0.0; // This can only occur ife2 is large compared to other terms. Setting w2=0 implicitly reduces e2. There is Alb resulting energy discrepancy due to
// Alb limitation on sublimation and latent heat flux. This is ignored because once the snow is gone energy computations are not pertinent.
}
QMs=MR*Rho_w*H_f;
Us2 = Us+Ae-QMs*dt; // redundant most of the time but recalc due to exceptions
}
// Check that nothing went wrong
if(MR < 0)
{
cout<<"Error - negative melt rate in snow"<<endl;
getchar();
}
if(Ws2 < 0)
{
cout<<"Error - negative w2 in snow"<<endl;
getchar();
}
Q = Ae/dt-QMs;
// Now set first pass values equal to final values to fake the averages below #$%^****take?
QMs1 = QMs;
Mr1 = MR;
Q1 = Q;
}
}
if(snowdgtvariteflag3 == 1)
{
//if( niter == 1)
cout<<endl<<"Iteration in pred-cor: niter, Us2, Ws2, Ts, Q, FM: "<<endl;
cout<<" "<<(niter-1)<<" "<<Us2<<" "<<Ws2<<" "<<TSURFs<<" "<<Q<<" "<< FM<<endl;
}
} //while ((abs(Ws2-Ws1) > wtol || abs(Us2-Us1) > utol) && (niter < imax)) //go to 1
Ws = Ws2;
Us = Us2;
// average values from two time steps for output. This is done for MR and e to ensure mass balance and the others for better physical comparisons
QHs = (QHs+QHs1)* 0.5;
QEs = (QEs+QEs1)* 0.5;
Es = (Es+Es1)* 0.5;
MR = (MR+Mr1)* 0.5;
QMs = (QMs+QMs1)* 0.5;
TSURFs = (TSURFs+TSURFs1) * 0.5;
Qnet = (Qnet + Qnet1) * 0.5;
Q = (Q+Q1) * 0.5;
smelt = (smelt+smelt1) * 0.5/(H_f*Rho_w); //cdgt 5/4/04 surface melt smelt .convert from energy KJ/m^2/hr to water depth m/hr of melt.
return;
}
//*************************************************************************
// CALCULATE CANOPY MASS FLUX AT ANY INSTANT
void QFMc(float Us, float Ws, float Wc, float A, float dt, float rid, float P, float Pr, float Ps, float Ta, float V, float RH, float Qsi, float atff, float Qli,
float cosZen, float EmC, float Ems, float *param, float *sitev, int iradfl, float Qnetob, int iTsMethod, float *mtime,
// Following variables are output
float &Tc, float &QHc, float &QEc, float &Ec, float &Qpc, float &Qps, float &Qmc, float &Mc, float &FMc, float &intc,float &Inmax, float &ieff, float &Ur, float &Cf, float &Taufb,
float &Taufd, float &Qsib, float &Qsid, float &Taub, float &Taud, float &Qsnc, float &Qsns, float &Qlnc, float &Qlns, float &Rkinc, float &Rkinsc, float &Vz, float &TSURFs, float &Tac,
// Just for testing
float &tave, float &qnet, float &QHs, float &QEs, float &Es, float &MR, float &QMs, float &Q, float &FM, float &refDepth, float &totalRefDepth, float &Smelt, float &smeltc )
{
float TAK, TAVEK, RHOA, rhom, fKappaS, ds, TherC, Zs, Zm,Fs, Qp, Qc1, Qc2 ;
float d, Z0c, Rimax, Rcastar, var_a, var_b, fkappaS, Betab,Betad, Qlis, Ess, Esc, QH, QE, E;
float Tssk, Tck;
//not used-but not deleted yet
//#$%____6.11.13
float Hcan, Ac;
// DOUBLE PRECISION Ur
//yjs Constant data set
//common /tsk_save/ tssk_old, tsavek_old, Tsavek_Ave, Tssk_ave
// Parameters
Ems=param[2]; // emmissivity of snow [nominally 0.99],
float cg =param[3], // Ground heat capacity [nominally 2.09 KJ/kg/C],
z=param[4], // Nominal meas. height for air temp. and humidity [2m],
zo=param[5], // Surface aerodynamic roughness [m],
rho=param[6], // Snow Density [Nominally 450 kg/m^3],
rhog=param[7], // Soil Density [nominally 1700 kg/m^3],
lc=param[8], // Liquid holding capacity of snow [0.05],
ks=param[9], // Snow Saturated hydraulic conductivity [160 m/hr],
de=param[10], // Thermally active depth of soil [0.4 m],
abg=param[11], // Bare ground albedo [0.25],
avo=param[12], // Visual new snow albedo [0.95],
anir0=param[13], // NIR new snow albedo [0.65],
lans= param[14], // the thermal conductivity of fresh [dry], snow [0.0576 kJ/m/k/hr],
lang= param[15], // the thermal conductivity of soil [9.68 kJ/m/k/hr],
wlf= param[16], // Low frequency fluctuation in deep snow/soil layer [1/4 w1 = 0.0654 radian/hr],
rd1= param[17], // Apmlitude correction coefficient of heat conduction [1],
fstab=param[18], // Stability correction control parameter 0 = no corrections, 1 = full corrections
Tref=param[19], // Reference temperature of soil layer in ground heat calculation input
dNewS=param[20], // The threshold depth of for new snow [0.001 m],
gsurf=param[21], // The fraction of surface melt that runs off [e.g. from a glacier],
// cdgt gsurf added for modeling surface runoff from a glacier
// Site variables
df = sitev[0], // Drift factor
Apr = sitev[1], // Atmospheric Pressure [Pa],
qg = sitev[2], // Ground heat flux [KJ/m^2/hr], This is more logically an
Cc = sitev[4], // Canopy Coverage
LAI = sitev[6]; // Leaf Area Index
//the following is passed to INTERCEPT instead of param(27)==param[26], same for cc
float Uc = param[26]; // Unloading rate coefficient (Per hour) (Hedstrom and pomeroy, 1998)
// To ensure all temperatures in kelvin
TAK = Ta + T_k;
TAVEK = tave + T_k;
RHOA = Apr / (Ra_g*TAK); // Density of Air in kg/m3 ifAPr in Pa
rhom = lc * rho;
// Some computations for conductivity
fKappaS = lans/(rho*C_s); // lans= lamda= thermao conductivity
ds = sqrt(2 * fKappaS /W1da_y); // fkappas =k= diffusivity
TherC = lans /(ds * rd1 *rho *C_s); // In QFM, related to thermal conductivity , lambda, of snow (Rs in Ori)
Zs = Ws * Rho_w/rho; // snow depth
//yjs save the old values
float tave_old = tave;
float EA = svpw(Ta) *RH; // The saturation vapour pressure over water is used
// because most instruments report relative humidity relative to water.
// Fraction of snow on canopy [Dickinson et. al (1993) eqn (50a)]
if(Inmax == 0.) //(When LAI is zero for open area model)
Fs= 0.0;
else
Fs = pow((Wc/Inmax),(2.0/3));
if(Fs > 1)
Fs=1;
INTERCEPT(Ta, LAI, P, Wc, dt, Inmax, Uc, Cc, ieff,Ur,intc);
/*param[26] = Uc;
sitev[4] = Cc;*/
// Total heat advected by precipitation is
Qp = QPF(Pr,Ta, T_0, Ps,Rho_w, H_f, C_w, C_s);
// Heat advected by precipitaion on canopy snow and sub-canopy snow is
if(P > 0)
{
if(Wc > 0)
{
Qpc = intc/P * Qp; // Energy from precipitaiton that hits the canopy snow
Qps = Qp - Qpc; // Energy advected by precipitaion that passes through canopy gap and thoroughfall from canopy
}
else
{
Qpc = 0.0;
Qps = ((P - intc)/P) * Qp;
}
}
else
{
Qpc = 0.0;
Qps = 0.0;
}
tave = TAVG (Us,Ws, Rho_w, C_s, T_0, rhog, de, cg, H_f);
//cout<<tave<<endl;
//yjs as described as below, the original UEB does not consider the refreezing. in this
// change, the model will consider the refreezing effect starting from the top to the bottom.
// Here is the predictor.
//yjs the method is: refreezing can be modeled ifthe Us is greater than 0.0 without any precipiation,
// meanwhile the total refreezing depth in the snowpack is less than the Refreezing depth times the daily damping of wet snow.
// if(Wc.EQ.0.and.p.EQ.0.) THEN // When there is no snow in the canopy
// Tc = Ta
// ELSE
// Tc = 0.0 // First assume snow is melting and then ifresult is negative - calculate canopy temperature having determined snow is not melting
// ENDIF
//********** To Calculate Refr Depth
if( (Us > 0) && (Ps <= 0) && (Pr <= 0) && (totalRefDepth <= rd1*ds) && (Ws > 0))
{
Qc1= QcEst(Ws,P,T_k,Tck,V,Zm,d,Z0c,Rimax,Rcastar,Cf,Fs, Qli,Hcan,Vz,Ta,RH,Rkinsc,Qps,T_0,Ps,Qsi,atff,cosZen, Apr,TAK, EA, A, Ac, Wc,Inmax, Qnetob,iradfl,param,sitev );
Qc2= QcEst(Ws,P,T_k -0.01,Tck,V,Zm,d,Z0c,Rimax,Rcastar,Cf,Fs, Qli,Hcan,Vz,Ta,RH,Rkinsc,Qps,T_0,Ps,Qsi,atff,cosZen, Apr,TAK, EA, A, Ac,Wc,Inmax, Qnetob,iradfl,param,sitev );
Grad(Qc1,Qc2,0.0,-0.01, var_a, var_b);
refDepth = refDep(lans,var_a, var_b, H_f, rhom, dt, refDepth); //refreezing depth
}
else
refDepth=0.0;
// call Temperature
TSURFs= SRFTMPSC (Tssk, Us,Ws,Wc,A,dt,P,Pr,Ps,Ta,V,RH,Qsi,atff,Cf, Qli,cosZen,EmC,Ems,param,sitev,iradfl,Qnetob,iTsMethod,mtime,
Qpc,Qps, Inmax, Rkinc,Rkinsc,Vz,Tc,T_k,TAK,EA,RHOA, fkappaS,rho,TherC,Fs, tave,refDepth,Smelt, smeltc); // This will give me Tsurf, Tc, and smeltc
//cout<<TSURFs<<endl;
if(iradfl != 1) // if iradfl==1 Go to 13 // To avoid these steps ifthe net radiation is input
{
PSOLRAD(Qsi,atff,param,Cf,Taufb,Taufd,Qsib,Qsid); // Output variables:
TRANSRADCAN (cosZen,sitev,param, Betab,Betad,Taub,Taud); // Output variables:
NETSOLRAD(Ta,A,Betab,Betad,Wc,Taub,Taud, Qsib,Qsid,param,Fs, Qsns,Qsnc ); // Output: Qsns,Qsnc (Net subcanopy, canopy solar radiation)
NETLONGRAD(RH,Ta,TSURFs,Tc,T_k,Fs,EmC,Ems,SB_c,Cf,sitev, Qli,param, Qlis,Qlns,Qlnc ); // Output: Qsns,Qsnc
}
/*13*/Ess = svpi(TSURFs);
Esc = svpi(Tc);
TURBFLUX(Ws,Wc,A,T_k,Tc,Ta,TSURFs,RH,V,EA,P,param,sitev, d,Z0c,Vz,Rkinc,Rkinsc,Tac,Fs,Ess,Esc, QHc,QEc,Ec,QHs,QEs,Es,QH,QE,E);
INTERCEPT(Ta,LAI,P,Wc,dt,Inmax,Uc,Cc, ieff,Ur,intc); // Output variables
// melt from the canopy
Qmc = smeltc;
Mc = Qmc/(Rho_w*H_f);
// Ridistribution of intercepted snow subtracting in mass balancep
// We are applying same amount as unloading is lost from the canopy from the wind redistribution
// Rid = Ur
//***************** UPDATING THE MASS BALANCE AT CANOPY
/*12*/ FMc = intc-Ec-Mc-Ur;
//***************** UPDATING THE MASS and ENERGY BALANCE AT SUB-CANOPY
MR = FMELT(Us,Rho_w,Ws,H_f,lc, rid,ks,Pr); //yjs Add a fraction to reduce the evaporation after snow gone // MR in m/hr
QMs = MR*Rho_w*(H_f+(tave-T_0)*C_w); // Include advection of
// meltwater/rain that is at tave so that the model does not
// crash when there is no snow and it rains.
// QMs in kj/m2/hr
// dgt 5/4/04 Add surface melt that runs off to melt runoff and melt energy so that energy and mass balances
// are still correct
MR = MR + Smelt/(H_f*Rho_w)*gsurf;
QMs=QMs+Smelt*gsurf;
if(iradfl == 0)
// QNET = QSI*(1.0-A)+QLNET
qnet = Qsns+Qlns; // At sub canopy snow
else
qnet = Qnetob;
// if(Ws.EQ.0.and. p.EQ.0.) THEN // vinod added to orgi UEB
// Es = 0.
// MR = 0.
// ENDIF
Q = qnet + Qps + qg + QHs + QEs-QMs;
FM =1.0*(Pr+Ps)-intc +Ur +Mc -MR -Es; // int,ur,Mc added here
return;
}
//************************* SRFTMP () *********************************
// COMPUTE THE SURFACE TEMPERATURE OF SNOW
float SRFTMPSC (float &Tssk,float Us,float Ws,float Wc,float A,float dt,float P,float Pr,float Ps,float Ta,float V,float RH,float Qsi,float atff,float cf,float Qli,float cosZen,
float EmC,float Ems,float *param,float *sitev,int iradfl,float Qnetob,int iTsMethod,float *mtime,float Qpcin,float Qpsin,float Inmax,float Rkinc,float Rkinsc,float Vz,
float &Tc,float Tk,float &Tak,float &EA,float &RHOA,float &fkappaS,float &RHO,float &TherC,float &Fs,float &Tave,float &refDepth,float &smelt,float &smeltC
)
{
float F1, F2, F1ts,F1tc,F2ts,F2tc,J11, J12, J21, J22, delTs, delTc, SRFTMPSC_v;
float S1num, S2num, S1denom, S2denom; //
float Tssk1 , Tck1 , Tss, Tck , S1, S2, Tclast, Tslast, ERc, ER;
float Tlb, Tub, Flb, Fub;
int iterC, ibtowrite = 0;
float Tssk1p, Tck1p;
float TSURFs;